US12174331B1 - Projection-based embedded discrete fracture model using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method - Google Patents
Projection-based embedded discrete fracture model using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method Download PDFInfo
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Definitions
- the present invention relates to the field of reservoir numerical simulation technology, especially to a novel projection-based embedded discrete fracture model using hybrid of TPFA and MFD method.
- MFE mixed finite element method
- MFD mimetic finite difference method
- the purpose of the present invention is to provide a novel projection-based embedded discrete fracture model (DFM) using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method
- the novel pEDFM constructed by this model can deal with anisotropic reservoirs with full permeability tensor, TPFA-MFD (or MFD) is implemented in the pEDFM framework for the first time, which significantly extends the original generic pEDFM using TPFA to become a special case of the new pEDFM in the case of K-orthogonal grids, and significantly expands the application scope of the pEDFM framework.
- the present invention provides a novel projection-based embedded discrete fracture model using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method, which includes the following steps:
- letf 1 be a low-conductivity fracture
- its permeability and fracture width are k f and w f , respectively
- the fracture grid in pEDFM adopts the transmissibility based on TPFA
- three types of connections are affected by low-conductivity fractures:
- Cont 1 eff Cont 1 ⁇ Cont 1 0 (6)
- step S2 let a number set of the matrix grid which is adjacent to the matrix grid m i be neigh m i , then the set of effective connections on each m i -side face of m i is:
- a T is a distribution matrix of the numerical flux on each surface of m i to the flux on each connection in Cont 2 eff (m i ).
- flux i A T flux i (9)
- step S3 the flux on each connection related to m i , is calculated by using the transmissibility matrix given in Eq. (14), and the discrete scheme of the continuity equation in m i is obtained.
- a transmissibility is in a simple scheme based on TPFA
- the effective connection Cont 2 eff (f j ) related to f j includes f-f connection Cont f j f-f and m-f connection Cont f j m-f
- the set of fracture grids adjacent to f j reflected from Cont f j f-f is denoted as neigh f j
- the discrete scheme of the continuity equation in f j is:
- each matrix grid is obtained, the transmissibility of all effective m-m-connections and m-f-connections matrix grids is known, while a transmissibility of fracture grids in m-f connections still adopts a simple scheme based on TPFA.
- the present invention adopts a novel projection embedded DFM using the hybrid method of TPFA and MFD, and its technical effects are as follows:
- FIG. 1 is a model diagram
- FIG. 2 is a sketch of some cases
- FIG. 3 is a Cartesian background grid corresponding to the reservoir model and the reservoir model of example 1;
- FIG. 4 shows a water saturation distribution at 200 days calculated by different methods in case 1 of the example 1;
- FIG. 5 shows a water saturation distribution at 200 days calculated by different methods in case 2 of the example 1;
- FIG. 6 is a pressure distribution of 200 days calculated by different methods in case 2 of the example 1;
- FIG. 7 is a water cut curve of production wells in case 1 and case 2 of the example 1;
- FIG. 8 is a distribution of water saturation at 200 days calculated by different methods in case 2 of the example 2;
- FIG. 9 shows a pressure distribution at 200 days calculated by different methods of the example 2.
- FIG. 10 is a water cut curve of production wells calculated by different methods of the example 2.
- FIG. 11 is a reservoir model and grid of the new pEDFM and DFM of the example 5.
- FIG. 12 shows a water saturation and pressure distribution after 400 days and 600 days obtained by different calculation methods of the example 5.
- FIG. 13 is a comparison of water saturation and pressure distribution after 200 days and 600 days obtained by different calculation methods in case 2 of the example 5.
- v ⁇ is the flow velocity
- q ⁇ ,sc is the source and sink term of phase a under the ground condition
- S ⁇ and B ⁇ are the saturation and volume coefficient of phase a, respectively
- t is time
- ⁇ porosity
- K is the permeability tensor
- ⁇ ⁇ is the mobility of phase ⁇
- p ⁇ , k r ⁇ , ⁇ ⁇ and B ⁇ are the pressure, relative permeability, viscosity and volume coefficient of phase ⁇ , respectively.
- k ra , ij ⁇ k ra ( S a , j ) if ⁇ F i ⁇ ⁇ ⁇ 0 k ra ( S a , i ) if ⁇ F i ⁇ ⁇ ⁇ 0 ( 7 )
- T i ⁇ ⁇ ⁇ " ⁇ [LeftBracketingBar]" ⁇ ⁇ i ⁇ ⁇ ⁇ " ⁇ [RightBracketingBar]” ⁇ K i ⁇ r i ⁇ ⁇ ⁇ " ⁇ [LeftBracketingBar]” r i ⁇ ⁇ ⁇ " ⁇ [RightBracketingBar]” 2 ⁇ n i ⁇ ⁇ , r i ⁇ is a vector from grid i-center to grid, ⁇ i ⁇ -center, n i ⁇ is the unit outward normal vector of ⁇ i ⁇ , and p i ⁇ is the pressure value at the center of ⁇ i ⁇ .
- the transmissibility matrix T i given by MFD is generally more denser than that given by TPFA, which is different from the diagonal transmissibility matrix in (10).
- X i (x i1 ⁇ x i , L, x i ⁇ ⁇ x i , L, x in i ⁇ x i ) T
- x i is the vector of the center of grid i
- x i ⁇ is the position vector of ⁇ i ⁇ center
- N i (
- d is the grid dimension
- a i diag(
- Q i orth(A i X i )
- TPFA is a form of MFD in the case of K-orthogonality without adding additional pressure degrees of freedom to the connection between grids, however, in the case of non-K orthogonal, the definition of additional pressure degree of freedom is difficult to avoid. With the additional pressure degree of freedom, there will be a flux continuity condition, so that the global equations can still be solved in a closed form.
- TPFA can be used to estimate the numerical flux on K-orthogonal grids, for example, it has a regular grid of isotropic permeability, while MFD-based flux approximation is used only in the remaining grids that do not satisfy K-orthogonality.
- Eq. (5), Eq. (6), Eq. (10) and Eq. (12) the discrete scheme of Eq. (3) can be obtained as follows:
- Eq. (13) and Eq. (15) constitute the global equations, and the Newton-Raphson (NR) iteration method is used to solve the equations to obtain the pressure, saturation distribution and production dynamic data.
- NR Newton-Raphson
- the EDFM mainly includes three types of connections, namely, the connections between two adjacent matrix grids, the connections between the matrix grid and the inter-grid fracture it contains, and the connection between inter-grid fractures.
- the connections between two grids are denoted by ( ⁇ , ⁇ ).
- the first type of connection includes (m i , m j ) and (m i , m k )
- the second type of connection includes (m i , f i ), (m j , f j ) and (m k , f k )
- the third type of connection includes (f i , f k ).
- the first case is the connection between inter-grid fractures on the same fracture surface.
- the transmissibility is calculated as:
- the second case is the connection between multiple fracture grids that may exist in the same matrix grid, which is generally calculated by star-delta transformation.
- pEDFM is a model between EDFM and DFM, as shown in FIG. 1 ( b ) , taking f; as an example, pEDFM projects f i along the x and y directions to 1 ij and 1 ik , respectively, at this time, pEDFM transforms the original model in FIG. 1 ( a ) into the model in FIG. 1 ( c ) .
- the corresponding flow area is the projection area of f i meanwhile, since the connection of (m j , f i ) and (m k , f i ) occupies the area of 1 ij and 1 ik , the flow area of the original (m j , f i ) and (m k , f i ) is weakened. Meanwhile, because f i and f j are projected onto 1 ij , there is also a connection between f i and f j .
- the core idea of the generic pEDFM workflow is to use the micro-translation projection method to deal with high-conductivity fracture units, and to use the non-projection transmissibility multiplier method to model low-conductivity fractures.
- the permeability of the m-f connections added to the pEDFM in FIG. 1 is:
- the transmissibility of the original m-f connections is weakened. Taking (m i , f i ) as an example, the transmissibility is calculated as:
- the generic pEDFM gives a non-projection method to model low-conductivity fractures, as shown below:
- the updated transmissibility of the connection is:
- connection between the matrix and the fracture in EDFM is very simple, and only the connection between the matrix grid and the fracture grid contained in the matrix grid is established, it is essentially a local dual-medium model, which makes the m-f connections in EDFM not affect the original m-m connections between adjacent matrix inter-grid. Therefore, when using MFD to deal with the full tensor permeability of the matrix grid in EDFM, it is only necessary to use the transfer matrix based on dense MFD in the structured background matrix grid to replace the diagonal transmissibility matrix obtained by TPFA in the original matrix grid. Of course, it can be further considered that the permeability of the matrix grid is the influence of the full tensor case on the m-f transmissibility in EDFM.
- m contains a fracture unit f i , m i and m j are adjacent, in EDFM, the pressure is continuous on the intersection I ij of m i and m j , this facilitates the application of the aforementioned MFD theory to construct flux continuity conditions at I ij .
- the essence of pEDFM is to project fractures onto the interface of matrix grids, the original embedded discrete scheme is transformed into an approximate DFM to deal with.
- pEDFM as shown in FIG.
- the f i in the matrix grid m i needs to be projected on I ij , but not fully covered I ij , the area covered by the fracture projection is denoted as I ij 1 , the remaining region on the I ij plane is I ij 2 , the pressure is continuous only on the m i -side and m j -side of I ij 2 , the pressure on the m i -side and m i -side of I ij 1 may be discontinuous, for example, if the permeability of the fracture is only slightly higher than that of the matrix grid, at this time, fluid is displaced to m j , from m i , and there is a pressure difference that cannot be ignored on both sides of I ij 1 . Therefore, the pressure values on different connections may be distributed on the intersection of the matrix grids that undertake the fracture projection in pEDFM, and it is necessary to distinguish the possible discontinuous pressures on the left and right sides on
- the pressure degree of freedom is only added to the effective connection related to the matrix grid. Since TPFA can still be used to calculate the numerical flux in the fracture. Therefore, the transmissibility information of the f-f connections in the generic pEDFM workflow can be kept unchanged without the need to define additional pressure degrees of freedom on the original f-f connections to carry out MFD. In other words, by obtaining effective m-m connections and m-f connections, an additional pressure degree of freedom is defined only on these effective connections related to the matrix grid.
- the additional degree of freedom added for the connection is judged to be located on the m side of 1.
- the pressure degree of freedom is located on both sides of I ij . In general, it is based on the matrix grid in the connection to solve the pressure degree of freedom added to the connection on which side of the corresponding matrix grid surface is located.
- the average pressure on the side of the matrix grid surface close to the matrix grid surface should be used (it should be noted that, as mentioned above, the matrix grid surface may have different average pressures on two sides of the matrix grid surface).
- the average pressure is a weighted average of the additional pressure degrees of freedom added by each effective connection on the side of the matrix grid surface near the matrix grid with the corresponding flow area as the weight.
- the average pressure p 1 ij m i of the side near m i of 1 ij and the average pressure p 1 ij m i of the side near m, of 1 are calculated as follows:
- the additional pressure degree of freedom p (m i , f i ) is considered to be on the side of 1 ij near m i .
- 1 ij m i be the side of 1 ij near m i
- 1 ij m j is the side of 1 ij near m j .
- the effective connection set associated with 1 ij m i as a set of connections in which the added pressure degree of freedom in Cont 1 eff is located in 1 ij m i , noting Cont 1 eff (1 ij m i ), the flow area of the corresponding connection and the increased pressure degree of freedom are A ⁇ and p ⁇ , respectively, ⁇ Cont 1 eff (1 ij m i ).
- the increased pressure degree of freedom of the original m-f connection may fall on two substrate grids, such as f i in FIG.
- the outward normal flux on one side of the grid is also related to the pressure on other sides of the grid. Therefore, the average pressure p ij i on one side of the matrix grid is defined to participate in the calculation of the outward normal flux on the side of the matrix grid based on MFD and the calculation is as follows:
- the generic pEDFM uses the transmissibility multiplier method to deal with low-conductivity fractures, so that pEDFM can generally model various low-conductivity fractures.
- the transmissibility multipliers are based on the harmonic average scheme in TPFA, and the transmissibility of each connection affected by the low-conductivity fractures is updated with the transmissibility of the low-conductivity fractures.
- Let f l be a low-conductivity fracture, and its permeability and fracture width are k f and w f , respectively.
- the fracture grid in the pEDFM of the invention still adopts the transmissibility based on TPFA
- the connection affected by low-conductivity fractures is divided into the following three treatment methods according to different connection types:
- T f i ⁇ f j ( T f i ⁇ f j - 1 + T f l - 1 )
- T f l k f l ⁇ A ( f i , f j ) w f l / 2 ( 30 )
- the transmissibility matrix T m i in m i is calculated by using the Eq. (9) based on TPFA, if not, then the transmissibility matrix T m i in m i is calculated by using the MFD-based Eq. (12).
- the efficient connections Cont 2 eff (f j ) related to f j include f-f connections (Cont fj f-f ) and m-f connections (Cont fj m-f ), the set of fracture grids adjacent to f j reflected from Cont fj f-f is denoted as neigh f j , then the discrete scheme of the continuity equation in f j can be written as Eq. (40). It should be emphasized that the reason why the form of the mass transfer part corresponding to the f-f connections in Eq.
- the pressure degrees of freedom of the new pEDFM include n m matrix grid center pressure, n f fracture grid average pressure, and n c additional pressure degrees of freedom, a total of n m +n f +n c
- the degree of freedom of water saturation includes n m matrix grid average saturation and n f fracture grid average saturation, a total of n m +n f , therefore, the global degree of freedom is 2(n m +n f )+n c .
- the global equations include a continuity equation of 2n m matrix grids (including oil phase and water phase, and therefore 2n m , not n m ), that is also the Eq. (39), the continuity equation of n f fracture grids (including oil phase and water phase), namely Eq. (40), and n c flux continuity conditions composed of Eq. (42) and Eq. (44), Therefore, the global equations are also 2(n m +n f )+n c , and it can be closed solution.
- the nonlinear solver based on Newton-Raphson (NR) iteration is used to solve the global equations to obtain the pressure and water saturation distribution at each time.
- FIGS. 3 ( a ) and ( b ) show two reservoir models in this case, in which the first model contains only one high-conductivity fracture consistent with the coordinate line, and the second model has an additional flow barrier. There is a water injection well and a production well in the lower left corner and the upper right corner of the reservoir respectively.
- FIGS. 3 ( c ) and ( d ) show the Cartesian background grid of the two models.
- the reservoir permeability is the anisotropic permeability tensor of the principal axis in the x and y directions in Eq. (45).
- the relative permeability function is shown in Eq. (46), and the other physical parameters are shown in table 1.
- FIG. 4 compares the water saturation distribution at 200 days calculated by LGR, new pEDFM, EDFM and DFM at case 1.
- FIG. 5 and FIG. 6 compare the water saturation and pressure distribution at 200 days calculated by LGR, new pEDFM, EDFM and DFM at case 2, respectively.
- FIG. 7 compares the water cut curves of production wells in case 1 and case 2. It can be seen that the new pEDFM can achieve almost the same saturation, pressure distribution and well response results as LGR and DFM.
- EDFM produces significant errors when simulating two-phase flow across high-conductivity fractures in case 1.
- the flow barrier in case 2 did not prevent the flow of injected water in EDFM, and the pressure distribution calculated by EDFM did not reflect the discontinuity of pressure on both sides of the flow barrier.
- the dynamic data of oil wells calculated by EDFM are also significantly different from the reference solution. The analysis of the results of this example shows that the new pEDFM can effectively solve the limitations of EDFM in the applicability of flow scenarios.
- FIG. 8 and FIG. 9 compare the water saturation and pressure distribution at 200 days calculated by pEDFM using TPFA, new pEDFM, and EDFM using MFD, respectively.
- FIG. 10 compares the water cut curves of production wells calculated by different methods.
- the new pEDFM can obtain almost the same calculation results as the reference solution, and the calculated water flooding front and pressure distribution accurately reflect the principal axis direction of the permeability tensor in Eq. (47) (i.e., the angle with the coordinate axis is 30 degrees).
- the pEDFM using TPFA can simulate the blocking effect of the flow barrier on the flow, the difference with the reference solution is still very obvious. From the calculated water drive front and pressure distribution, it can be seen that the use of TPFA to estimate the numerical flux leads to its failure to accurately grasp the principal axis direction of the permeability tensor in Eq.
- the reservoir model of this implementation case contains 36 high-conductivity fractures marked with solid lines and 4 flow barriers marked with dotted lines.
- the permeability of anisotropic reservoir is the full permeability tensor in Eq. (47).
- the initial pressure and reference pressure of the reservoir are both 20 MPa.
- the other physical parameters are the same as those in table 1, and the relative permeability data are the same as that in Eq. (46).
- FIGS. 13 ( c ) and ( d ) show the matching grid used by DFM and the non-matching grid used by the new pEDFM, respectively. It can be seen that when generating the matching grid for the complex fracture network, a large number of small grids will be generated in the narrow area between the fractures, so that the number of generated grids is large and the generation of grids is difficult. Practice shows that in the case of more complex fracture grids, even some mature triangular (tetrahedral) grid generation software cannot generate grids that match the geometric structure of the fracture network.
- FIG. 12 and FIG. 13 compare the water saturation and pressure distribution after 400 days and 600 days calculated by DFM and new pEDFM in case1 and case 2, respectively. It can be seen intuitively that the new pEDFM can achieve the same calculation accuracy as DFM in case1 and case 2. It is shown that the new pEDFM is more practical than the DFM for implementations with complex grids.
- the present invention adopts a projection embedded DFM based on the hybrid method of TPFA and MFD, wherein the new pEDFM can deal with anisotropic reservoirs with full permeability tensor.
- TPFA-MFD or MFD
- the implementation of TPFA-MFD is realized in the pEDFM framework, which significantly expands the original generic pEDFM using TPFA as a special case of the new pEDFM in the case of K-orthogonal grids, and significantly expands the application scope of the pEDFM framework.
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Abstract
This invention presents a projection embedded discrete fracture model integrating a TPFA and MFD hybrid approach, creating a pEDFM framework for various anisotropic two-phase flow situations. It specifies the distribution of extra pressure freedoms on matrix grids for MFD implementation, maintains f-f connections in TPFA through a standard pEDFM workflow, and introduces a low-conductivity fracture treatment for MFD. It also outlines the derivation of numerical flux calculation formulas for effective m-m and m-f connections. The mixed TPFA-MFD design applies to numerical flux estimation across both K-orthogonal and non-K-orthogonal grids, enhancing computational efficiency and facilitating the spatial discretization of continuity equations for matrix and fracture grids under anisotropic permeability conditions. A global equation system is formulated based on the continuity of effective connections, with time discretization via the implicit backward Euler method and pressure and water saturation distributions determined by a Newton-Raphson based nonlinear solver.
Description
The present invention relates to the field of reservoir numerical simulation technology, especially to a novel projection-based embedded discrete fracture model using hybrid of TPFA and MFD method.
In the past 20 years, the flow simulation of fractured formation has been a hot topic. Since the flow is usually dominated by fracture systems with complex geometries, a clear geometric description of the large-scale fracture network is required to ensure the simulation accuracy. So far, there are two widely used modeling methods. One is the discrete-fracture model (DFM) based on conforming grids. The model uses unstructured grids to match the fracture geometry, so that the fracture is located on the intersection surface between the matrix grids. Various DFMs have been developed using different numerical methods to discretize the governing equations. The DFMs constructed by different numerical methods have differences in accuracy, efficiency and adaptability of flow types.
However, as of now, an efficient and robust pEDFM framework applicable to general anisotropic two-phase flow scenarios has not yet been proposed. In practice, when using a generic pEDFM workflow that can be applied to a wide range of flow scenarios, the details of the inter-grid connections and the treatment of low-conductivity fractures in pEDFM will become much more complex than in the original pEDFM, which also brings challenges to the development of a pEDFM framework that can be applied to a wide range of anisotropic two-phase flow scenarios. In cases of non-K-orthogonal grids caused by anisotropy, the mixed finite element method (MFE) and the mimetic finite difference method (MFD) are allowed to directly use the pressure of the centroid of the grid surface to approximate the gird-surface flux it is more suitable for fractured reservoirs where there may be discontinuous distribution of physical quantities in space, and has been widely studied in recent years. Since MFE generally uses Raviart-Thomas (RTO) basis function, in the case of poor grid quality, the calculation accuracy will decrease, but it has been proved that MFD can achieve higher accuracy than MFE in the case of irregular grid distribution and poor grid quality. In 2016, Yan et al. constructed an MFD-based EDFM, demonstrating the effect of implementing MFD in EDFM to process full permeability tensors, but due to the inherent limitations of EDFM, the MFD-based EDFM will have significant errors in common actual flow scenarios such as blocking fractures or multiphase flow crossing fractures. In 2017, Zhang et al. developed a multi-scale MFD-based EDFM. Abushaikha and Terekhov in 2020, Zhang and Abushaikha in 2021, Li and Abushaikha in 2021 developed a fully implicit reservoir simulation framework based on MFD, applied and improved the framework to DFM and complex reservoir compositional models, respectively. However, compared with TPFA, MFD increases the density of the Jacobian matrix of the global equations, which increases the computational cost and reduces the computational efficiency. Therefore, in 2023, Dong et al. constructed a hybrid method of TPFA and MFD (TPFA-MFD) for fault block reservoirs, the hybrid method uses TPFA to estimate the numerical flux for K-orthogonal grids in the MFD framework, to reduce the density of Jacobian matrix and improving the computational efficiency. Previous pEDFMs requires extra manual treatments to achieve its theoretical computational advantage due to the lack of generic algorithm to construct fracture projection configurations and various inter-grid connections. Rao et al., (2023) proposed a first easy-programming generic pEDFM workflow to achieve its computational superior than DFM and EDFM in general cases without manual treatments, which laid the algorithm foundation for its commercialization. However, there is no method to combine the generic pEDFM workflow with TPFA-MFD.
The purpose of the present invention is to provide a novel projection-based embedded discrete fracture model (DFM) using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method, the novel pEDFM constructed by this model can deal with anisotropic reservoirs with full permeability tensor, TPFA-MFD (or MFD) is implemented in the pEDFM framework for the first time, which significantly extends the original generic pEDFM using TPFA to become a special case of the new pEDFM in the case of K-orthogonal grids, and significantly expands the application scope of the pEDFM framework.
To achieve the above purpose, the present invention provides a novel projection-based embedded discrete fracture model using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method, which includes the following steps:
-
- s1. constructing a treatment method suitable for low-conductivity fractures when using MFD;
- s2. constructing a numerical flux calculation method for effective m-f and m-m connections, the hybrid TPFA-MFD method is used to estimate the numerical flux on each effective connection related to K-orthogonal and non-K-orthogonal grids by TPFA and MFD, respectively, and the spatial discretization of the continuity equation of the matrix grid and the fracture grid in the case of anisotropic full permeability tensor is realized;
- s3. constructing global equations by combining the flux continuity conditions of effective m-f and m-m connections, the time discretization scheme of implicit backward Euler scheme is adopted, and the nonlinear solver based on Newton-Raphson method is used to calculate the distribution of pressure and water saturation.
Preferably, in step s1, letf1 be a low-conductivity fracture, its permeability and fracture width are kf and wf, respectively, the fracture grid in pEDFM adopts the transmissibility based on TPFA, and three types of connections are affected by low-conductivity fractures:
(1) for f-f connections, set to fi and fi, a transmissibility of fi-fj before being affected by f is:
T fi f j =(T f i −1 +T f j −1)−1 (1)
wherein, Tfi is a transmissibility of fracture grid fi, Tfj is a transmissibility of fracture grid fj;
T f
wherein, Tfi is a transmissibility of fracture grid fi, Tfj is a transmissibility of fracture grid fj;
-
- a transmissibility of (fi, fj) affected by f1 is:
-
- wherein, kfi is a permeability of fracture grid f1, wfi is an opening of fracture grid f1, A(fi, fj) is a flow area of (fi, fj);
- if other low-conductivity fractures that affect the f-f connections exist, using the Eq. (1) to continue updating;
- (2) for m-f connections, set to mi and fi, suppose that a transmissibility of fj in mi-fj connections not affected by fl is based on the Tfj, the effect of fl is applied to fj, which is equivalent to the series connection of low-conductivity fractures fl and fj, that is, the transmissibility of fj is updated as:
T fj =(T fj −1 +T fi −1) (3) - if other low-conductivity fractures that affect the m-f connections exist, using Eq. (3) to continue updating Tfj;
- (3) for m-m connections, set to mi and mj, the mi-mj connections are split into mi-fl connections and mj-fl connections, the flow area of mi-fj connections and mj-fl connections are the flow area A(mi, mj) of (mi, mj), wherein a transmissibility of fl is:
-
- wherein, A(mi, mj) is a flow area of (mi, mj);
- if other low-conductivity fractures fk that affect (mi, mj) exist, a transmissibility of fl is updated by using a transmissibility of fk in Eq. (3):
Preferably, a treatment of low-conductivity fractures will add new connections in Cont1 eff, and an updated Cont1 eff is recorded as Cont2 eff.
Cont1 eff=Cont1−Cont1 0 (6)
Cont1 eff=Cont1−Cont1 0 (6)
-
- wherein, Cont1 is a inter-grid connection set obtained by ignoring the low-conductivity fractures when using the generic pEDFM to treat the low-conductivity fractures with the non-projection transmissibility multiplier method; Cont1 0 is a set of connections with a flow area of 0 in Cont1; and Cont1 eff is the efficient set in Cont1.
Preferably, in step S2, let a number set of the matrix grid which is adjacent to the matrix grid mi be neighm i , then the set of effective connections on each mi-side face of mi is:
according to Eq. (7):
-
- wherein
p 1ij mi is an average pressure of the side near mi of intersecting face of mi and mj, pζ is a pressure degree of freedom added by the ζ connection in Cont2 eff(1ij mi ), pζ is a flow area of the ζ connection in Cont2 eff(1ij mi ); - the conversion formula between the average pressure of mi-side of mi-side faces and the value of the pressure degree of freedom added by each connection in Cont2 eff(mi) is obtained:
p mi =Ap mi (8) - wherein
p mi is a column vector composed ofp ij mi , (j∈neighmi ), pmi is a column vector composed of pj(j∈Cont2 eff(mi)), each j-line of A represents the area weight when using Eq. (7) to calculate the average pressure on the j-th mi-side face of mi.
- wherein
Preferably, in step S2, AT is a distribution matrix of the numerical flux on each surface of mi to the flux on each connection in Cont2 eff(mi).
fluxi =A Tflux i (9)
fluxi =A T
-
- firstly, it is judged whether the matrix grid mi is K orthogonal, if yes, then the transmissibility matrix Tm
i in mi is calculated by using the Eq. (10) based on TPFA;
- firstly, it is judged whether the matrix grid mi is K orthogonal, if yes, then the transmissibility matrix Tm
-
- wherein Tβ,γ m
i represents β row and η column of matrix Tmi , riβ is a vector from grid i-center to grid ∂Ωiβ-center, niβ is the unit outward normal vector of ∂Ωiβ, piβ is the pressure value at the center of ∂Ωiβ; - if not, then the transmissibility matrix Tm
i in mi is calculated by using Eq. (11) based on MFD;
- wherein Tβ,γ m
-
- wherein, Ωi is a control region of matrix grid mi, |Ωi| is a volume of matrix grid T mi, Ki is a permeability tensor of matrix grid mi, Xi=(xi1−xi, L, xiβ−xi, L, xin
i −xi)T, xi is a vector of the center of grid i, xiβ is a vector of ∂Ωiβ center, Ni=(|Ωi1|ni1, L, |∂Ωiβ, niβ, L, |∂Ωini |nini )T, d is a grid dimension, Ai=diag(|Ωi1, L, |∂Ωiβ, L, |∂Ωini ), Qi=orth(AiXi). - then, the average pressure is used to participate in the calculation of the numerical flux on each surface of the matrix grid, and it is obtained that:
flux i =T mi p mi =T mi Ap mi =T mi A(p mi I=p mi ) (12) - wherein, fluxi is a column vector composed of numerical flux on each surface of the matrix grid, each j-line of A represents the area weight when the average pressure of the j-th surface of mi side calculated by Eq. (28), meanwhile, AT is the distribution matrix of the numerical flux on each surface of mi to the flux on each connection in Contz (ma) and I is a column vector wherein one of elements is 1 and the length is the effective connection number of the matrix grid;
- furthermore, by combining Eq. (9) and Eq. (12), get:
fluxi =A T T mi A(p mi I-p mi ) (13) - for the matrix grid mi, the actual transmissibility matrix is:
=A T T mi A (14).
- wherein, Ωi is a control region of matrix grid mi, |Ωi| is a volume of matrix grid T mi, Ki is a permeability tensor of matrix grid mi, Xi=(xi1−xi, L, xiβ−xi, L, xin
Preferably, in step S3, the flux on each connection related to mi, is calculated by using the transmissibility matrix given in Eq. (14), and the discrete scheme of the continuity equation in mi is obtained.
-
- wherein, krα,ij is a relative permeability of the α-th phase between the matrix grid mi and the matrix grid mj according to the single-point upwind scheme, μα,ij ij and Bα,ij are the viscosity and volume coefficient of the ith phase calculated by the arithmetic average scheme between the matrix grid mi and the matrix grid mj, respectively, subscript β refers to the serial number of the intersection surface of matrix grid mi and matrix grid mj in all surfaces of matrix grid mi, Fiβ is the outward normal flux of matrix grid mi on the β-th plane, is the β-th row and γ-th column of the transmissibility matrix Tm
i , and piγ is the surface center pressure of the γ-th plane of the matrix grid mi, pi is the body center pressure of matrix grid pi, Δt is the time stepping, ϕi, Sα,i and Bα,i are the porosity of matrix grid mi, the saturation of a phase and the volume coefficient of a phase, respectively, and the superscripts t+Δt and t represent the time;
- wherein, krα,ij is a relative permeability of the α-th phase between the matrix grid mi and the matrix grid mj according to the single-point upwind scheme, μα,ij ij and Bα,ij are the viscosity and volume coefficient of the ith phase calculated by the arithmetic average scheme between the matrix grid mi and the matrix grid mj, respectively, subscript β refers to the serial number of the intersection surface of matrix grid mi and matrix grid mj in all surfaces of matrix grid mi, Fiβ is the outward normal flux of matrix grid mi on the β-th plane, is the β-th row and γ-th column of the transmissibility matrix Tm
For a fracture grid fj, a transmissibility is in a simple scheme based on TPFA, the effective connection Cont2 eff(fj) related to fj includes f-f connection Contf j f-f and m-f connection Contf j m-f, the set of fracture grids adjacent to fj reflected from Contf j f-f is denoted as neighf j , then the discrete scheme of the continuity equation in fj is:
Preferably, when each matrix grid is obtained, the transmissibility of all effective m-m-connections and m-f-connections matrix grids is known, while a transmissibility of fracture grids in m-f connections still adopts a simple scheme based on TPFA.
-
- for m-m connections, suppose mi and mk, then:
fluxmi →mk =(p mi I−p mi )fluxmk →mi =(p mi I−p mi ) (17) - the corresponding flux continuity conditions are:
(p mi I-p mi )+(p mi I−p mi )=0 (18)
- for m-m connections, suppose mi and mk, then:
For m-f connections, suppose mi and fj, then:
fluxmi →f j =(p m i I−p m i )fluxf j →m i =T f j (p f j −p (m i ,f j )) (19)
fluxm
For f-f connections, the transmissibility formula in generic pEDFM without defining additional pressure degrees of freedom is adopted.
Therefore, the present invention adopts a novel projection embedded DFM using the hybrid method of TPFA and MFD, and its technical effects are as follows:
-
- (1) The concepts of effective connection and average pressure on the matrix grid surface are defined, and the distribution of additional pressure degrees of freedom is clarified. A low-conductivity fracture treatment method suitable for MFD is proposed. The numerical flux calculation formula of each effective connection is derived, and the flux conservation conditions of each effective connection are given, and the implementation of MFD or TPFA-MFD in pEDFM is realized.
- (2) The novel pEDFM of the present invention essentially includes pEDFM using MFD and pEDFM using TPFA, the present invention demonstrates through theory and implementation examples that pEDFM using TPFA-MFD can achieve almost the same calculation accuracy as pEDFM using MFD, but pEDFM using TPFA-MFD can use TPFA to estimate the numerical flux of K-orthogonal grids, not all using MFD, which improves the structure of the Jacobian matrix when solving global equations and improves the calculation efficiency.
- (3) The novel pEDFM can achieve the same calculation accuracy as DFM, and can avoid the difficulty of generating matching grids by DFM and the additional computational cost caused by the over-density of local grids caused by the narrow area between fractures, and has good convergence.
- (4) Compared with several commonly used numerical simulation frameworks for fractured reservoirs, the new pEDFM has better comprehensive performance and has very significant field application potential.
The following is a further detailed description of the technical scheme of the invention through the drawings and embodiments.
In order to illustrate the technical effect of the invention, the existing technology and the improvement of the invention are explained first.
1.1 Reservoir Two-Phase Flow Control Equation
Continuity equation of each phase:
Wherein vα is the flow velocity, qα,sc is the source and sink term of phase a under the ground condition, Sα and Bα are the saturation and volume coefficient of phase a, respectively, t is time, ϕ is porosity.
The flow velocity satisfies the Darcy's law:
Wherein K is the permeability tensor, λα is the mobility of phase α, pα, krα, μα and Bα are the pressure, relative permeability, viscosity and volume coefficient of phase α, respectively.
Taking Eq. (2) into Eq. (1), get:
1.2 Discretization of Control Equations
Integrating both sides of Eq. (3) in grid i control volume Ωi and time period [t, t+Vt], get:
wherein ∫Ω
The rectangular formula is used to estimate the time integral on the left side and the space integral on the right side of Eq. (4), get:
By using the divergence theorem, the first term on the left side of (5) can be rewritten as follows:
-
- wherein, subscript iβ represents the βth edge of grid i (if it is three-dimensional, it is the βth surface of grid i), and Fiβ is the outward normal flux on ∂Ωiβ.
For two adjacent grids, it may be written as grid i and grid j, and the intersection of grid i and grid j is written as eij, ∃β, η s.t., ∂Ωiβ=∂Ωjη=eij. In Eq. (5), the single-point upstream weight scheme in (6) is generally used in krα, and μα and Bα generally adopt the arithmetic average scheme in Eq. (7).
2.1 Two-Point Flux Approximation (TPFA)
In the finite volume method with two-point flux approximation, the numerical flux of grid i on eij is calculated as:
-
- wherein
riβ is a vector from grid i-center to grid, ∂Ωiβ-center, niβ is the unit outward normal vector of ∂Ωiβ, and piβ is the pressure value at the center of ∂Ωiβ.
According to Eq. (8), the expression of the outward normal flux of ∂Ωiβ expressed by the transmissibility matrix Ti can be obtained:
-
- wherein, T denotes the β row and η columns of matrix Ti.
2.2 Simulating Finite Difference
- wherein, T denotes the β row and η columns of matrix Ti.
Generally, TPFA can only achieve high-precision flux approximation in K-orthogonal grids, and K-orthogonal meets that:
K i r iβ ×n iβ,=0 (11)
K i r iβ ×n iβ,=0 (11)
MFD can be applied to both K-orthogonal and non-K-orthogonal grids, the transmissibility matrix Ti given by MFD is generally more denser than that given by TPFA, which is different from the diagonal transmissibility matrix in (10).
In MFD, the calculation expression of Ti is:
Wherein Xi=(xi1−xi, L, xiβ−xi, L, xin i −xi)T xi is the vector of the center of grid i, xiβ is the position vector of ∂Ωiβ center, Ni=(|∂Ωi1|ni1, L, |∂Ωiβ|niβ, L, |∂Ωin i |nin i )T, d is the grid dimension, Ai=diag(|∂Ωi1|, L, |∂Ωiβ|, L, |∂Ωin i |)) Qi=orth(AiXi)
2.3 Flux Continuity Conditions
It can be seen from 2.1 and 2.2 that grid i and grid j have an outward normal flux Fiβ and Fjη on the intersection eij, respectively, the flux continuity condition should be satisfied, that is, the algebraic sum of Fiβ and Fjη should be equal to 0.
In fact, when using TPFA, piβ can be eliminated according to Eqs. (9) and (13), the numerical flux based on TPFA can be calculated as Eq. (14), that is, the transmissibility formula based on the harmonic average scheme in the common TPFA, in essence, there is no need to add additional pressure degrees of freedom between grid i and grid j.
It can be considered that TPFA is a form of MFD in the case of K-orthogonality without adding additional pressure degrees of freedom to the connection between grids, however, in the case of non-K orthogonal, the definition of additional pressure degree of freedom is difficult to avoid. With the additional pressure degree of freedom, there will be a flux continuity condition, so that the global equations can still be solved in a closed form.
2.4 Hybrid of TPFA and MFD
TPFA can be used to estimate the numerical flux on K-orthogonal grids, for example, it has a regular grid of isotropic permeability, while MFD-based flux approximation is used only in the remaining grids that do not satisfy K-orthogonality. According to Eq. (5), Eq. (6), Eq. (10) and Eq. (12), the discrete scheme of Eq. (3) can be obtained as follows:
The Eq. (13) and Eq. (15) constitute the global equations, and the Newton-Raphson (NR) iteration method is used to solve the equations to obtain the pressure, saturation distribution and production dynamic data.
(3) EDFM and Generic pEDFM Workflow
3.1 EDFM
EDFM mainly includes three types of connections, namely, the connections between two adjacent matrix grids, the connections between the matrix grid and the inter-grid fracture it contains, and the connection between inter-grid fractures. In order to facilitate the description, the connections between two grids are denoted by (·, ·). As shown in FIG. 1(a) , the first type of connection includes (mi, mj) and (mi, mk), the second type of connection includes (mi, fi), (mj, fj) and (mk, fk), and the third type of connection includes (fi, fk).
For the first type of connection, taking (mi, mj) as an example, when TPFA is used, similar to Eq. (14), it can be calculated that the transmissibility of (mi, mj) is half of the harmonic mean of the transmissibility of mi and the transmissibility of mj:
-
- wherein A(·) denotes the area operator and 1ij is the interface of mi and mj.
Similarly, for the second type of connection,
For the third type of connection, it is generally necessary to subdivide it into two cases. The first case is the connection between inter-grid fractures on the same fracture surface. For example (fi, fk), the transmissibility is calculated as:
The second case is the connection between multiple fracture grids that may exist in the same matrix grid, which is generally calculated by star-delta transformation.
3.2 Generic pEDFM Process
pEDFM is a model between EDFM and DFM, as shown in FIG. 1(b) , taking f; as an example, pEDFM projects fi along the x and y directions to 1ij and 1ik, respectively, at this time, pEDFM transforms the original model in FIG. 1(a) into the model in FIG. 1(c) . At this point, compared with EDFM, fi needs to be connected to mj and mk, the corresponding flow area is the projection area of fi meanwhile, since the connection of (mj, fi) and (mk, fi) occupies the area of 1ij and 1ik, the flow area of the original (mj, fi) and (mk, fi) is weakened. Meanwhile, because fi and fj are projected onto 1ij, there is also a connection between fi and fj.
The core idea of the generic pEDFM workflow is to use the micro-translation projection method to deal with high-conductivity fracture units, and to use the non-projection transmissibility multiplier method to model low-conductivity fractures.
When the matrix permeability is isotropic, the permeability of the m-f connections added to the pEDFM in FIG. 1 is:
-
- wherein fi,1
ij p and fj,1ij p are the projections of fi and fj on 1ij.
- wherein fi,1
The transmissibility of the original m-m connections is reduced to:
By halving the transmissibility of the matrix grid, the transmissibility of the original m-f connections is weakened. Taking (mi, fi) as an example, the transmissibility is calculated as:
Added transmissibility (fi, fi):
Then, the generic pEDFM gives a non-projection method to model low-conductivity fractures, as shown below: the updated transmissibility of the connection is:
Wherein Tij′ and Ti are the updated and original transmissibility of the connection; connected updated and original transmissive semi-transmissibility of low-conductivity fractures; kf and wf are the permeability and pore size of low-conductivity fractures, respectively; Aij is the flow cross-sectional area corresponding to the connection; if kf=0, the updated transmissibility in Eq. (25) will become zero, so the flow barrier can block the flow. It should be noted that if multiple low-conductivity fractures intersect with the same connection, the transportability of the connection will be updated multiple times by using Eq. (25).
4.1 the Basic Idea of the Present Invention
The connection between the matrix and the fracture in EDFM is very simple, and only the connection between the matrix grid and the fracture grid contained in the matrix grid is established, it is essentially a local dual-medium model, which makes the m-f connections in EDFM not affect the original m-m connections between adjacent matrix inter-grid. Therefore, when using MFD to deal with the full tensor permeability of the matrix grid in EDFM, it is only necessary to use the transfer matrix based on dense MFD in the structured background matrix grid to replace the diagonal transmissibility matrix obtained by TPFA in the original matrix grid. Of course, it can be further considered that the permeability of the matrix grid is the influence of the full tensor case on the m-f transmissibility in EDFM. In general, due to the simplicity of the grid connection structure in EDFM, it is a simple task to construct an EDFM based on MFD. However, pEDFM, which performs better than EDFM, has a much more complex connection relationship than EDFM. The most important point is that the m-f connections in pEDFM will weaken the original m-m connections, or even directly cover the original m-m connections and make them disappear, which makes the above strategies that can work in EDFM not directly work in pEDFM. The specific explanation is as follows:
As shown in FIG. 2(a) , m, contains a fracture unit fi, mi and mj are adjacent, in EDFM, the pressure is continuous on the intersection Iij of mi and mj, this facilitates the application of the aforementioned MFD theory to construct flux continuity conditions at Iij. However, because the essence of pEDFM is to project fractures onto the interface of matrix grids, the original embedded discrete scheme is transformed into an approximate DFM to deal with. In pEDFM, as shown in FIG. 2(b) , the fi in the matrix grid mi needs to be projected on Iij, but not fully covered Iij, the area covered by the fracture projection is denoted as Iij 1, the remaining region on the Iij plane is Iij 2, the pressure is continuous only on the mi-side and mj-side of Iij 2, the pressure on the mi-side and mi-side of Iij 1 may be discontinuous, for example, if the permeability of the fracture is only slightly higher than that of the matrix grid, at this time, fluid is displaced to mj, from mi, and there is a pressure difference that cannot be ignored on both sides of Iij 1. Therefore, the pressure values on different connections may be distributed on the intersection of the matrix grids that undertake the fracture projection in pEDFM, and it is necessary to distinguish the possible discontinuous pressures on the left and right sides on the intersection of the matrix grids.
The above analysis gives the following important inspirations:
i) The concept of effective connectivity needs to be introduced. As shown in FIG. 2(c) , the projection of fracture fj on Iij will completely cover Iij, at this time, there will be no need to define additional pressure degrees of freedom between mi and mj. If the additional definition is given, the global equations will not have the flow continuity equation related to the pressure degree of freedom, so that the global equations can not be solved in closed form. Therefore, it is necessary to introduce the definition of effective connection, that is, the connection whose actual flow area is not 0. Only such a connection can define an additional pressure degree of freedom.
ii) The pressure degree of freedom is only added to the effective connection related to the matrix grid. Since TPFA can still be used to calculate the numerical flux in the fracture. Therefore, the transmissibility information of the f-f connections in the generic pEDFM workflow can be kept unchanged without the need to define additional pressure degrees of freedom on the original f-f connections to carry out MFD. In other words, by obtaining effective m-m connections and m-f connections, an additional pressure degree of freedom is defined only on these effective connections related to the matrix grid.
iii) The distribution of the pressure degree of freedom on which side of the matrix grid surface should be solved. As mentioned above, the essence of pEDFM is to project the fracture onto the interface of the matrix grid, and transform the original embedded discrete scheme into an approximate DFM to deal with. Therefore, the added pressure degrees of freedom can be considered to be distributed on the matrix grid surface. Meanwhile, because the pressure on both sides of the fracture projection area on the matrix grid surface may no longer be continuous, the pressure degrees of freedom added by different connections need to be distinguished to which side of the matrix grid surface is located. As shown in FIG. 2(b) , the projection area of fracture fj on Iij is not 0, therefore, there are two effective connections of (mi, fi) and (mj, fi). Then the pressure degree of freedom added for (mi, fi) is actually located on the side of Iij near m, side, the pressure degree of freedom added for (mj, fi) is actually located on the side of Iij near mj side, and the values of these two pressure degrees of freedom are generally different. Therefore, for an effective m-f connection, if the fracture f is projected on the interface 1 of the matrix grid, the additional degree of freedom added for the connection is judged to be located on the m side of 1. For an effective (mi, mj) connection, the pressure degree of freedom is located on both sides of Iij. In general, it is based on the matrix grid in the connection to solve the pressure degree of freedom added to the connection on which side of the corresponding matrix grid surface is located.
(iv) The concept of average pressure on the matrix grid surface needs to be introduced. Since the pressure on the grid surface is needed to obtain the MFD flow operator in the matrix grid, pEDFM is different from EDFM as mentioned above. It may have multiple connections on the matrix grid surface, not only the m-m connections in EDFM, but also the original m-m connections may be completely replaced by other m-f connections. At this time, if the value of the pressure degree of freedom added to the different connections is subdivided on each grid surface to participate in the construction of the transmissibility matrix based on MFD in the matrix grid, the complexity of the algorithm will be significantly increased and the robustness and practicability of the algorithm will be reduced. Therefore, when constructing the transmissibility matrix based on MFD in the matrix grid, the average pressure on the side of the matrix grid surface close to the matrix grid surface should be used (it should be noted that, as mentioned above, the matrix grid surface may have different average pressures on two sides of the matrix grid surface). The average pressure is a weighted average of the additional pressure degrees of freedom added by each effective connection on the side of the matrix grid surface near the matrix grid with the corresponding flow area as the weight. As shown in FIG. 2(b) , the average pressure p 1 ij m i of the side near mi of 1ij and the average pressure p 1 ij m i of the side near m, of 1 are calculated as follows:
-
- wherein, p(m
i , fi ), p(mj , fi ) and p(mi , mj ), and are the pressure degrees of freedom added for (mi, fi), (mj, fi) and (mi, mj), respectively, A(mi , fi ), A(mj , fi ) and A(mi , mj ) are the corresponding flow areas of (mi, fi), (mj, fi) and (mi, mj), respectively. It can be seen that the pressure on the left and right sides of 1ij 1. is discontinuous, the average pressure on the left and right sides of 1ij is no longer continuous. Of course, if there is no fracture projection on the matrix grid surface, the average pressure on both sides of 1ij can be calculated to be continuous, which degenerates into the case in EDFM.
4.2 Basic Concepts
Concept 1: effective connection
- wherein, p(m
Since the generic pEDFM workflow adopts the non-projection processing method of transmissibility multiplier for low-conductivity fractures, this section first ignores low-conductivity fractures, and at this time, the connection set between grids Cont1 can be obtained, the transmissibility of the corresponding connection is calculated according to Eq. (19) to Eq. (25), and the corresponding flow area is also reflected in these transmissibility calculation formulas. In Cont1, the set of connections with flow area of 0 is Cont1 0, it can be seen that the transmissibility of the connection in Cont1 0 must be 0, and it has no effect on the results of simulation calculation. Taking FIG. 2 as an example, C(mi, mj)∈Cont1 0, therefore, the effective set in definition Cont1 is Cont1 eff.
Cont1 eff=Cont1−Cont1 0 (27)
Cont1 eff=Cont1−Cont1 0 (27)
Concept 2: Cont1 eff (1i j m i ) and the corresponding pressure degree of freedom
It can be seen from the basic theory of MFD in 2.2, since the permeability of fracture grip is generally isotropic, when pEDFM is constructed based on MFD, there is no need to change the original f-f connections and the corresponding transmissibility in Cont1 eff. However, the permeability of the matrix grid may be in the full tensor form, so it is necessary to construct an additional pressure degree of freedom for each m-m and f-m connection in Cont1 eff. As mentioned above, pEDFM essentially projects the fracture grid in the matrix grid to the intersection surface of the matrix grid to form an approximate DFM to deal with. It can be considered that each m-m and f-m effective connection increases. A pressure degree of freedom is located on the matrix grid surface associated with the connection. For example, (mi, fi) in FIG. 2(b) , The additional pressure degree of freedom p(m i , f i ) is considered to be on the side of 1ij near mi. Let 1ij m i be the side of 1ij near mi, 1ij m j is the side of 1ij near mj. Then, it is possible to define the effective connection set associated with 1ij m i as a set of connections in which the added pressure degree of freedom in Cont1 eff is located in 1ij m i , noting Cont1 eff (1ij m i ), the flow area of the corresponding connection and the increased pressure degree of freedom are Aζ and pζ, respectively, ζ∈Cont1 eff (1ij m i ). It should be pointed out that the increased pressure degree of freedom of the original m-f connection may fall on two substrate grids, such as fi in FIG. 2(c) , it is due to the projection in the x direction and they direction, respectively, therefore, (fi, mi)∈Cont1 eff (1ij m i ) and (fi, mi)∈Cont1 eff (1ik m i ), the corresponding flow area should not be fracture area, but A(fi,1 ij p) and A(fi,1 ik p), respectively.
Concept 3: Average Pressure of Matrix Grid Surface
From the MFD theory of 2.2, it can be seen that in the case of full permeability tensor, the outward normal flux on one side of the grid is also related to the pressure on other sides of the grid. Therefore, the average pressure p ij i on one side of the matrix grid is defined to participate in the calculation of the outward normal flux on the side of the matrix grid based on MFD and the calculation is as follows:
4.3 Treatment of Low-Conductivity Fractures
As described in 3.2, the generic pEDFM uses the transmissibility multiplier method to deal with low-conductivity fractures, so that pEDFM can generally model various low-conductivity fractures. The transmissibility multipliers are based on the harmonic average scheme in TPFA, and the transmissibility of each connection affected by the low-conductivity fractures is updated with the transmissibility of the low-conductivity fractures. Let fl be a low-conductivity fracture, and its permeability and fracture width are kf and wf, respectively. Considering that the fracture grid in the pEDFM of the invention still adopts the transmissibility based on TPFA, the connection affected by low-conductivity fractures is divided into the following three treatment methods according to different connection types:
-
- i) for f-f connections, it may be set to fi and fj, and the fi-fj transmissibility before being affected by fl is:
T fi fj =(T fi −1 +T fj −1)−1 (29) - then the transmissibility affected by fl is:
- i) for f-f connections, it may be set to fi and fj, and the fi-fj transmissibility before being affected by fl is:
-
- wherein, A(f
i , fj ) is the flow area of (fi, fj). - if there are other low-conductivity fractures that affect the connection, then the Eq. (29) continues to be updated.
- ii) For m-f connections, it may be set to mi and fj, suppose that a transmissibility off in the mi-fj connections is not affected by fl, the original transmissibility of fj is based on the TPFA's Tf
j , the influence of fl is applied to fj, which is equivalent to connecting the low-conductivity fracture fl with fj in series, that is, the transmissibility off is updated as:
T fj =(T fj −1 +T fl −1)−1 (31) - if there are other low-conductivity fractures that affect the mi-fj connections, then use Eq. (31) to continue to update Tf
j . - iii) for m-m connections, it may be set to mi and fj, since there is no fracture grid available for the harmonic averaging scheme, it is necessary to split the mi-mj connections into two m-f connections, they are mi-fl and mj-fl respectively, and the flow area of these two connections is (mi, mj) flow area A(m
i , mj ), wherein the transmissibility off is:
- wherein, A(f
If there are other low-conductivity fractures (such as fk), then the transmissibility off is updated with the transmissibility of fk by Eq. (31), that is:
It can be seen that the treatment of low-conductivity fractures in this section will add new connections in Cont1 eff, and the updated Cont1 eff is recorded as Cont2 eff.
4.4 Numerical Flux Calculation of Effective Connection
Let the number set of the matrix grid which is adjacent to the matrix grid mi be neighm i , then the set of effective connections on each side of mi near mi is:
according to Eq. (28), the conversion formula between the average pressure of each side of mi near mi and the value of pressure degree of freedom added by each connection in Cont1 eff (mi) can be obtained as follows:
-
- wherein
p mi is a column vector composed ofp ij mi (j∈neighmi ), pmi is a column vector composed of pj(j∈Cont2 eff (mi)), each j row of A represents the area weight when the average pressure of the jth surface of mi near mi is calculated by Eq. (28), meanwhile, AT is the distribution matrix of the numerical flux on each surface of mi to the flow on each connection in Cont1 eff(mi):
fluxi =A T√{square root over (fluxi)} (35)
- wherein
Firstly, it is judged whether the matrix grid mi is K orthogonal, if yes, then the transmissibility matrix Tm i in mi is calculated by using the Eq. (9) based on TPFA, if not, then the transmissibility matrix Tm i in mi is calculated by using the MFD-based Eq. (12). As mentioned above, the average pressure is used to participate in the calculation of the numerical flow on each surface of the matrix grid, so it can be obtained that:
flux i =T m i p m i =T m i Ap m i =T m i A(p m i I−p m i ) (36)
-
- wherein, I is a column vector, wherein one of the elements is 1 and the length is the number of effective connections of the matrix grid.
Furthermore, combining Eq. (35) and Eq. (36), it is obtained that:
fluxi =A T T mi A(p m i I−p m i ) (37)
fluxi =A T T m
Therefore, for the matrix grid, the actual transmissibility matrix is:
=A T T mi A (38)
4.4 Global Equation
=A T T m
4.4 Global Equation
By using the transmissibility matrix given in Eq. (38), the flux on each connection related to mi can be calculated, by taking into Eq. (15), the discrete scheme of the continuity equation in m; can be obtained:
For a fracture grid fj, its transmissibility still adopts a simple TPFA scheme, the efficient connections Cont2 eff (fj) related to fj include f-f connections (Contfj f-f) and m-f connections (Contfj m-f), the set of fracture grids adjacent to fj reflected from Contfj f-f is denoted as neighf j , then the discrete scheme of the continuity equation in fj can be written as Eq. (40). It should be emphasized that the reason why the form of the mass transfer part corresponding to the f-f connections in Eq. (40) is different from the form of the mass transfer part corresponding to the m-f connections is that: in this work, in order to reduce the computational cost and algorithm complexity, no additional pressure degree of freedom is added to the f-f connections. Therefore, the mass transfer corresponding to the f-f connections is directly expressed in a numerical flux expression similar to that in Eq. (14) using grid average pressure and TPFA.
Meanwhile, when of each matrix grid is obtained, the transmissibility of all effective m-m connections and m-f connections matrix grids is known, and the transmissibility of the fracture grid in the m-f connections is still based on the TPFA scheme. Therefore, the continuity conditions of each m-m connection and m-f connection in Cont2 eff can be given.
For m-m connections, suppose that is mi and mk, then:
fluxmi →m k =(p m i I−p m i ),fluxm k →m i =(p m i I−p m i ) (41)
fluxm
For m-f connections, suppose that is mi and fj, then:
The corresponding flux continuity condition is:
(p mi I−p m i )+T f j (p f j −p (m i ,f j ))=0 (44)
(p m
For f-f connections, because the present invention still uses the transmissibility formula in Eq. (18) and Eq. (24) without defining additional pressure degrees of freedom in the generic pEDFM, there is no additional flow continuity condition for f-f connections.
In general, let the reservoir calculation domain contain nm matrix grids and nf fracture grids, the number of m-m and m-f connections contained in Cont2 eff is nc. The pressure degrees of freedom of the new pEDFM include nm matrix grid center pressure, nf fracture grid average pressure, and nc additional pressure degrees of freedom, a total of nm+nf+nc, the degree of freedom of water saturation includes nm matrix grid average saturation and nf fracture grid average saturation, a total of nm+nf, therefore, the global degree of freedom is 2(nm+nf)+nc. The global equations include a continuity equation of 2nm matrix grids (including oil phase and water phase, and therefore 2nm, not nm), that is also the Eq. (39), the continuity equation of nf fracture grids (including oil phase and water phase), namely Eq. (40), and nc flux continuity conditions composed of Eq. (42) and Eq. (44), Therefore, the global equations are also 2(nm+nf)+nc, and it can be closed solution. The nonlinear solver based on Newton-Raphson (NR) iteration is used to solve the global equations to obtain the pressure and water saturation distribution at each time.
Table 1 Physical Parameters of Reservoir Model
| Physical parameters | The value | Physical parameters | The value |
| Original formation | 15 | MPa | Water phase viscosity | 0.6 mPa · s |
| pressure | |||
| Initial water saturation | 0.2 | Reference pressure | 15 MPa |
| Thickness | 5 | m | |
1 × 10−3 |
| coefficient | |||
| Matrix porosity | 0.12 | Water phase compressibility | 5 × 10−4 |
| coefficient | |||
| Fracture porosity | 0.4 | |
1 × 10−4 |
| coefficient |
| Fracture permeability | 100000 | | Fracture compressibility | 1 × 10−4 |
| coefficient |
| Fracture aperture | 0.01 | m | Oil phase volume coefficient | 1.0 |
| under reference pressure |
| Fracture permeability of | 0 | mD | Water phase volume coefficient | 1.0 |
| blocking fracture | under reference pressure | ||
| |
2 mPa · s | ||
At this time, the Cartesian grids are K-orthogonal, and the reference solution can be obtained by local grid refinement (LGR) and the finite volume method based on TPFA. FIG. 4 compares the water saturation distribution at 200 days calculated by LGR, new pEDFM, EDFM and DFM at case 1. FIG. 5 and FIG. 6 compare the water saturation and pressure distribution at 200 days calculated by LGR, new pEDFM, EDFM and DFM at case 2, respectively. FIG. 7 compares the water cut curves of production wells in case 1 and case 2. It can be seen that the new pEDFM can achieve almost the same saturation, pressure distribution and well response results as LGR and DFM. However, EDFM produces significant errors when simulating two-phase flow across high-conductivity fractures in case 1. The flow barrier in case 2 did not prevent the flow of injected water in EDFM, and the pressure distribution calculated by EDFM did not reflect the discontinuity of pressure on both sides of the flow barrier. The dynamic data of oil wells calculated by EDFM are also significantly different from the reference solution. The analysis of the results of this example shows that the new pEDFM can effectively solve the limitations of EDFM in the applicability of flow scenarios.
Keeping the reservoir model and physical parameters of case 2 in case 1 unchanged, only the permeability tensor in Eq. (46) is rotated by 30 degrees to obtain the full permeability tensor in Eq. (47). Theoretically, TPFA will not be able to obtain high-precision numerical flux approximation at this time. Taking the DFM solution based on MFD as the reference solution, FIG. 8 and FIG. 9 compare the water saturation and pressure distribution at 200 days calculated by pEDFM using TPFA, new pEDFM, and EDFM using MFD, respectively. FIG. 10 compares the water cut curves of production wells calculated by different methods. It can be seen that: (i) the new pEDFM can obtain almost the same calculation results as the reference solution, and the calculated water flooding front and pressure distribution accurately reflect the principal axis direction of the permeability tensor in Eq. (47) (i.e., the angle with the coordinate axis is 30 degrees). (ii) Although the pEDFM using TPFA can simulate the blocking effect of the flow barrier on the flow, the difference with the reference solution is still very obvious. From the calculated water drive front and pressure distribution, it can be seen that the use of TPFA to estimate the numerical flux leads to its failure to accurately grasp the principal axis direction of the permeability tensor in Eq. (47), and mistakenly believe that the principal axis direction of the permeability tensor is x direction and y direction. (iii) The EDFM using MFD fails to effectively characterize the role of the flow barrier, which is also reflected in case 2 of the first case, but the numerical flux approximation based on MFD enables EDFM to simulate a water flooding front with an inclination of about 30 degrees on the left side of the high-conductivity fracture.
The above results demonstrate that the new pEDFM can achieve high-precision simulation results for the case with full permeability tensor, while the pEDFM using TPFA and the EDFM using MFD will have significant errors.
In this example, a more complex implementation example will be used to show the application effect of the new pEDFM, and to test that the new pEDFM can achieve the same calculation accuracy as DFM in the case of more complex slit network, and to show the advantages of the new pEDFM in grid generation compared with DFM. As shown in FIG. 11 , the reservoir model of this implementation case contains 36 high-conductivity fractures marked with solid lines and 4 flow barriers marked with dotted lines. The permeability of anisotropic reservoir is the full permeability tensor in Eq. (47). The initial pressure and reference pressure of the reservoir are both 20 MPa. The other physical parameters are the same as those in table 1, and the relative permeability data are the same as that in Eq. (46). Wherein, the injection-production wells in case1 are located in the lower left corner and the upper right corner of the reservoir, and the injection-production wells in case2 are located in the upper left corner and the lower right corner of the reservoir. FIGS. 13(c) and (d) show the matching grid used by DFM and the non-matching grid used by the new pEDFM, respectively. It can be seen that when generating the matching grid for the complex fracture network, a large number of small grids will be generated in the narrow area between the fractures, so that the number of generated grids is large and the generation of grids is difficult. Practice shows that in the case of more complex fracture grids, even some mature triangular (tetrahedral) grid generation software cannot generate grids that match the geometric structure of the fracture network.
Therefore, the present invention adopts a projection embedded DFM based on the hybrid method of TPFA and MFD, wherein the new pEDFM can deal with anisotropic reservoirs with full permeability tensor. For the first time, the implementation of TPFA-MFD (or MFD) is realized in the pEDFM framework, which significantly expands the original generic pEDFM using TPFA as a special case of the new pEDFM in the case of K-orthogonal grids, and significantly expands the application scope of the pEDFM framework.
Finally, it should be noted that the above implementation examples are only used to illustrate the technical scheme of the invention rather than to restrict it, although the invention is described in detail with reference to the better implementation example. The ordinary technical personnel in this field should understand that they can still modify or replace the technical scheme of the invention, and these modifications or equivalent substitutions can not make the modified technical scheme out of the spirit and scope of the technical scheme of the invention.
Claims (6)
1. A method for generating flow simulation of fracture formation, for an anisotropic media with full permeability tensor, by a projection-based embedded discrete fracture model (pEDFM) using a hybrid of two-point flux approximation (TPFA) method and mimetic finite difference (MFD) method, i.e., (TPFA-MFD) method, the method comprising:
discretizing of a generic fracture model of the anisotropic media, by a data processing system, for:
identifying a plurality of grids comprising matrix grids and fracture grids based on a location of each grid in the generic fracture model;
identifying three types of connections in a fracture network based on the location of each grid in the generic fracture model, wherein the three types of connections comprises:
m-m connection corresponding to connection between two matrix grids;
m-f connection corresponding to connection between a matrix grid and a fracture grid; and
f-f connection corresponding to a connection between two fracture grids; and
identifying effective m-m connections and/or effective m-f connections, wherein each effective m-m connection and/or each effective m-f connection comprises at least one low-conductivity fracture fl;
constructing a treatment method for each low-conductivity fracture by the data processing system, for:
identifying an inter-grid connection set Cont1 comprising a set of connections obtained from a generic pEDFM to treat the low-conductivity fractures with a non-projection transmissibility multiplier method is used that provides a flow area between adjacent grids, wherein the low-conductivity fractures are ignored;
identifying an efficient set of connections Cont1 eff based on the inter-grid connection set Cont1 as follows:
Cont1 eff=Cont1−Cont1 0 (6)
Cont1 eff=Cont1−Cont1 0 (6)
wherein Cont1 0 is a set of connections with a flow area 0 in the inter-grid connection set Cont1;
constructing a numerical flux calculation method for effective m-f and m-m connections, by the data processing system, for:
determining flux continuity conditions of effective m-f and m-m connections using the hybrid TPFA-MFD method, wherein the hybrid TPFA-MFD method comprises:
estimating a numerical flux on each effective m-f connection and/or effective m-m connection related to K-orthogonal grids using TPFA method; and
estimating a numerical flux on each effective m-f connection and/or effective m-m connection related to non-K-orthogonal grids using MFD method; and
performing a spatial discretization of a continuity equation of each matrix grid and each fracture grid in the effective m-m and m-f connections; and
constructing global equations, by the data processing system, by combining the flux continuity conditions of the effective m-f and m-m connections and a time discretization scheme of implicit backward Euler scheme, and calculating distribution of pressure and water saturation by solving the global equations using a nonlinear solver based on Newton-Raphson method.
2. The method for generating the flow simulation of fracture formation, for the anisotropic media with full permeability tensor, by the projection-based embedded discrete fracture model (pEDFM) using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method according to claim 1 , wherein the method for constructing the treatment method for each of the low-conductivity fractures by the data processing system comprises, determining a transmissibility of each fracture grid in pEDFM based on TPFA method, wherein the at least one low-conductivity fracture fl has a permeability kf and a fracture width wf, wherein determining transmissibility of fracture grids in the pEDFM includes determining the transmissibility in three types of connections that are affected by low-conductivity fractures, wherein the transmissibility based on low-conductivity fractures for the three types of connections are as follows:
(1) for f-f connections, set to connect between i-th fracture grid fi and j-th fracture grid fj, determining a transmissibility of fracture grids in fi-fj connection that is affected by low-conductivity fracture fl comprises:
determining a first transmissibility of fi-fj connection before being affected by the low-conductivity fracture grid fl as:
T fi f j =(T f i −1 +T f j −1) (1)
T f
wherein, Tf i is a transmissibility of fracture grid fi, Tfj is a transmissibility of fracture grid fj; and
determining a transmissibility of fi-fj connection after being affected by low-conductivity fracture f1 as:
wherein, kfi is a permeability of fracture grid f1, wfi is a width of an opening of fracture grid f1, A(f i , f j ) is a flow area of (fi, fj); and
updating the transmissibility Tf i f j using the Eq. (1) if other low-conductivity fractures fn that affect the f-f connections exist, wherein, for the low-conductivity fracture grid fn that intersects (fi, fj) connection, the transmissibility is further updated based on Equation (2) as:
(2) for m-f connections, set to connection between i-th matrix grid mi and j-th fracture grid fj, determining a transmissibility of fracture grid in mi-fj connection that is affected by low-conductivity fracture fj comprises:
identifying the transmissibility of j-th fracture grid fj in mi-fj connections not affected by low-conductivity fracture grid fl based on the transmissibility Tfj
obtaining the transmissibility Tfj of j-th fracture grid fj after applying the effect of low-conductivity fracture fl is-applied to the j-th fracture grid fj, which is equivalent to the series connection of low-conductivity fractures f1 and fj, wherein, the transmissibility Tfj of fracture grid fj is updated as:
T fj =(T f j −1 +T f l −1)−1 (3); and
T f
updating the transmissibility Td using Eq. (3) if other low-conductivity fractures fn that affect the mi-fj connections exist, wherein for the other low-conductivity fracture grid fn that intersect with mi-fj connection, the transmissibility Tfj is further updated based on Equation (3) as follows; and
(3) for m-m connections, set to connection between i-th matrix grid mi and j-th matrix grid mj, determining a transmissibility of fracture grid in the mi-mj connections that is affected by low-conductivity fracture fl comprises:
splitting the mi-mj connections into mi-fl connections and mj-fl connections, wherein, flow area of mi-fl connections and mj-fl connections is same as a flow area A(mi, mj) of (mi, mj), wherein a transmissibility of the low conductivity fracture fi is as follows:
and
updating the transmissibility Tfj of the low-conductivity fracture fl using Eq. (3) if other low-conductivity fractures fk that affect (mi, mj) exist, wherein the transmissibility of the low-conductivity fracture fl is updated by using a transmissibility of the other low-conductivity fracture fk in Eq. (3) as follows:
3. The method for generating flow simulation of fracture formation, for the anisotropic media with full permeability tensor, by the projection-based embedded discrete fracture model (pEDFM) using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method according to claim 1 , wherein constructing the numerical flux calculation method for the effective m-f and m-m connections, by the data processing system comprises:
identifying a number set of a matrix grid which is adjacent to a matrix grid mi to be neighm i , wherein a set of effective connections on each mi-side face of matrix grid mi is: Cont2 eff(mi)=j∈neigh m i ∪ Cont2 eff(lij m i ) according to Eq. (7):
wherein:
lij m i is the mi-side of lij, wherein lij; is the interface between matrix grid mi and matrix grid mj,
Cont2 eff(mi) denotes the set of connections in Cont2 eff that have additional pressure degree of freedom located on all mi-side faces of matrix grid mi in addition to Cont1 eff,
p l ij m i is an average pressure of a side near matrix grid mi on intersecting face of matrix grids mi and mj,
Cont2 eff(lij m i ) denotes the set of connections in Cont2 eff that have additional pressure degree of freedom is located on lij m i in addition to Cont1 eff,
pζ is a pressure degree of freedom added by ζth connection in Cont2 eff(lij m i ), and
Aζ is a flow area of the ζth connection in Cont2 eff(lij m i );
obtaining a conversion formula between the average pressure of mi-side of mi-faces and the value of the pressure degree of freedom added by each connection in Cont2 eff(mi) as follows:
p m i =Ap m i (8)
wherein:
p m i is a column vector composed of p ij m i (j∈neighm i ),
p ij m i is the average pressure of lij m i ,
pij m i , is a column vector composed of pj(j∈Cont2 eff(mi))
wherein, if j∈Cont2 eff, (mi) is a connection in Cont2 eff(mi), then pj denotes the added pressure degree of freedom for this connection, and
each j-line of A represents an area weight when using Eq. (7) to calculate the average pressure on lij m i (i.e., the mi-side of the j-th surface of mi).
4. The method for generating flow simulation of fracture formation, for the anisotropic media with full permeability tensor, by the projection-based embedded discrete fracture model (pEDFM) using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method according to claim 3 , wherein, constructing the numerical flux calculation method for the effective m-f and m-m connections, by the data processing system comprises:
using a distribution matrix AT to relate a numerical flux on each surface of mi denoted by fluxi to a numerical flux flux i on each effective connection in Cont2 eff(mi) as follows:
fluxi =A Tflux i (9),
fluxi =A T
wherein:
if the matrix grid mi is K orthogonal, then a transmissibility matrix Tm i in the i-th matrix grid mi is calculated by using Eq. (10) based on TPFA as follows:
wherein:
Tβ,γ m i represents β row and γ column of matrix Tm i ,
∂Ωiβ is portion of a control region of grid mi at β-th row and γ-th column of the transmissibility matrix Tβ,γ m i ,
|∂Ωiβ| is volume of the portion of the control region of grid mi at β-th row and γ-th column of the transmissibility matrix Tβ,γ m i ,
riβ is a vector from grid i-center to grid ∂Ωiβ-center, and
ηiβ is a unit outward normal vector of ∂Ωiβ; and
if the matrix grid mi is non-K orthogonal, then the transmissibility matrix Tm i in mi is calculated by using Eq. (11) based on MFD as follows:
wherein:
Ωi is a control region of matrix grid mi,
|Ωi| is a volume of matrix grid mi,
Ki is a permeability tensor of matrix grid mi,
Xi=(xi1−xi, . . . , xiβ−xi, . . . , xin i −xi)T,
xi is a vector of the center of grid i,
xiβ is a vector of ∂Ωiβcenter,
Ni=(|∂Ωi1|ηi1, . . . , |∂Ωiβ|ηiβ, . . . , |∂Ωin i |ηin i )T wherein Ni is the number of all the interfaces of the i-th grid,
d is a grid dimension,
tr denotes to calculate the trace of a matrix,
Ai=diag(|∂Ωi1|, . . . , ∂Ωin i |)), and
Qi=orth(AiXi) wherein Qi is a standard orthogonal basis for a column space of AiXi, wherein the number of columns in Qi is equal to the rank of AiXi;
using an average pressure to participate in the calculation of the numerical flux flux i on each surface of the matrix grid, as:
flux i =T m i p m i =T m i Ap m i =T m i A(p m i I−p m i ) (12)
wherein:
flux i is a column vector composed of numerical flux on each surface of the matrix grid,
each j-line of A represents the area weight when the average pressure on the mi-side of the j-th surface of mi is calculated by Eq. (8),
AT is a transverse of A and is a distribution matrix to relate the numerical flux on each surface of matrix grid mi to the flux on each connection in Cont2 eff(mi), and
I is a column vector with all elements being 1, and its length is equal to the number of effective connections in the matrix grid,
obtaining the numerical flux and actual transmissibility matrix on the matrix grid mi by combining Eq. (9) and Eq. (12), as follows:
fluxi =A T T mi A(p m i I−p m i ) (13),
fluxi =A T T m
wherein fluxi is the numerical flux on the matrix grid mi, and
for the matrix grid mi, the actual transmissibility matrix is:
{tilde over (T)} mi =A T T m i A (14).
{tilde over (T)} m
5. The method for generating flow simulation of fracture formation, for the anisotropic media with full permeability tensor, by the projection-based embedded discrete fracture model (pEDFM) using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method according to claim 4 , wherein constructing global equations by the data processing system comprises:
calculating the flow on each connection related to mi by using the actual transmissibility matrix given in Eq. (14), and obtaining a discrete scheme of the continuity equation in matrix grid mi as;
wherein:
krα,ij is a relative permeability of the α-th phase between the matrix grid mi and the matrix grid mj according to a single-point upwind scheme,
μα,ij and Bα,ij are viscosity and volume coefficient of the ith phase calculated by an arithmetic average scheme between the matrix grid mi and the matrix grid mj, respectively,
subscript β refers to a serial number of an intersection surface of matrix grid mi and matrix grid mj in all surfaces of matrix grid mi,
Fiβ is an outward normal flux of matrix grid mi on the β-th plane,
Tβ,γ m i is the β-th row and γ-th column of the actual transmissibility matrix {tilde over (T)}m i ,
is the surface center pressure of the γ-th plane of the matrix grid mi,
is a body center pressure of matrix grid mi,
Δt is a time stepping,
ϕi, Sα,i and Bα,i are a porosity of matrix grid mi, a saturation of α-th phase and the volume coefficient of α-th phase, respectively, and
superscripts t+Δt and t represent the time; and
obtaining a discrete scheme of continuity equation for the fracture grid fj, wherein when the transmissibility is in a simple scheme based on TPFA, the effective connection Cont2 eff(fj) related to fj includes f-f connection Contf j f-f and m-f connection Contf j m-f, and if the set of fracture grids adjacent to fj reflected from Contf j f-f is denoted as neighf j , then the discrete scheme of the continuity equation in fracture grid fj is:
6. The method for generating flow simulation of fracture formation, for the anisotropic media with full permeability tensor, by the projection-based embedded discrete fracture model using hybrid of two-point flux approximation and mimetic finite difference (TPFA-MFD) method according to claim 5 , wherein when actual transmissibility of each matrix grid {tilde over (T)}m i is obtained, the transmissibility of all matrix grids in effective m-m connections and m-f connections is known, while a transmissibility of fracture grids in m-f connections still adopts a simple scheme based on TPFA wherein:
for m-m connections, suppose mi and mk are matrix grids corresponding to i-th surface and k-th surface respectively, then,
the corresponding numerical flux is:
fluxmi →m k ={tilde over (T)} m i m k (p m i I−p m i )fluxm k →m i ={tilde over (T)} m i m k (p m i I−p m i ) (17)
fluxm
the corresponding flux continuity condition is:
{tilde over (T)} mi m k (p m i I−p m i )+{tilde over (T)} m i m k (p m i I-p m i )=0 (18)
{tilde over (T)} m
for m-f connections, suppose mi and fj are the matrix grid corresponding to i-th surface and the fracture grid corresponding to i-th surface respectively, then,
the corresponding numerical flux is:
fluxmi →f j ={tilde over (T)} m i f j (p m i I−p m i )fluxf j →m i =T f j (p f j −p (m i ,f j )) (19), and
fluxm
the corresponding flux continuity condition is:
{tilde over (T)} mi f j (p m i I−p m i )+T f j (p f j −p (m i ,f j ))=0 (20); and
{tilde over (T)} m
for f-f connections, the transmissibility is obtained using the generic pEDFM without defining additional pressure degrees of freedom is adopted.
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